Mesabi
Black is one of the varieties of coarse-grained (>2mm)
igneous rocks that formed in magma chambers in the rift. These
chambers formed at different depths >1-2 km deep in the rift.
They were the source for the surface lavas. Feeders from the magma
chambers to the lavas are called dikes when near vertical and sills
when
near horizontal. As magmas cooled in the deep chambers a variety
of minerals
crystallized and formed layers due to settling or flow giving rise
to “layered gabbros”. Because the Keweenawan rocks along
the North Shore are tilted to the east, erosion has exposed a cross
section of this system of rocks with lavas along the shore of Lake
Superior and the underlying intrusive feeders and magma chambers
away from the shore (the feeders are also found along the shore,
Silver Cliff is an example).

The exposed section also includes
sandstones that formed in shallow basins as rifting began,sandstones
interbedded
with the lavas which represent lulls in the volcanism during which
sediments derived from the lavas were deposited, and sandstones
which filled in the rift after volcanism ended. The brown and buff
colored
sandstones used for Pillsbury Hall across from CALA are an example
of the latter.

As mentioned by Dr. Weiblen, the anorthositic gabbro from Mesabi Black Quarry is related to the Proterozoic rift system that extends beneath the College of Design site at the University of Minnesota and is the reason this rock was selected for use in SITE INDEX.